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    Coccidia of the endangered South Island Takahē (Porphyrio hochstetteri) : investigations of pathobiology and management : a thesis presented in partial fulfilment of the requirements for the degree of Masters of Veterinary Science in Wildlife Health at Massey University, Manawatū, New Zealand
    (Massey University, 2018) Jolly, Megan Jayne
    The South Island Takahē (Porphyrio hochstetteri) is a large flightless rail, endemic to New Zealand currently listed as endangered with a population numbering approximately 340 individuals. The intensive management programme for this species has seen a modest increase in the population and includes strategies such as captive rearing for release at protected sites and numerous translocations of birds between these sites each year to maximise genetic diversity. This interconnectedness of geographically dispersed populations and critical points of high stocking density contribute to the potential for spread of infectious disease. Coccidian oocysts have been detected in Takahē faecal samples for decades and sporadically coccidia were implicated in the death of Takahē. By early 2015 concerns were being raised about markedly elevated individual faecal oocyst counts and the apparent failures of treatment with toltrazuril. The potential for significant negative impacts of coccidia in terms of both clinical disease and sub-clinical effects on juvenile growth rates and fertility led to the investigations reported in this thesis into the coccidia affecting Takahē. A novel Eimeria sp. is described from a Takahē host. Based on morphological characteristics this coccidian species is distinct from other Eimeria spp. described in hosts of the family Rallidae. A survey of stored historical faecal samples and contemporary routine screening samples demonstrated the presence of this Eimeria sp. across most of the fragmented conservation management network for Takahē. Modification of treatment protocols and management actions was closely associated temporally with a sustained reduction in the Eimeria sp. shedding rates at a breeding facility central to the Takahē population network. Preliminary results were supportive of the existence of a diurnal shedding pattern for the Eimeria sp. with a peak of oocyst shedding in the late afternoon after 3pm in winter, which has implications for the collection of screening samples and the interpretation of results collected at different times of day. Concurrent to these investigations into the biology of the Takahē coccidia, trials were carried out to establish the safety of the anti-coccidial medication, decoquinate, in Takahē. No clinically significant deleterious effects were found in the parameters examined. The findings presented are initial investigations into an Eimeria sp. from a Takahē host, the effectiveness of control measures implemented and safety of potential management options. The crisis of regular extreme oocyst counts in Takahē, which prompted this research, was resolved, however the potential for a recurrence is ever present in a species conservation programme that relies on intensive breeding and translocation of individuals. This research is the foundation for future research into the characterisation and management of Eimeria spp. in Takahē.
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    Geomorphology of the deglaciated Eglinton Valley, Fiordland : new insights into the origin of hummocky terrain : a thesis presented in partial fulfillment of the requirements for the degree of Master of Science in Geography at Massey University, Manawatu, New Zealand
    (Massey University, 2016) Walker, Goldie Sky
    The distribution and types of landforms within deglaciated valleys provide information on past processes and indicate the potential for future changes and associated hazards. This study is the rst to characterise the landform assemblages within Eglinton Valley, Fiordland, New Zealand, and develop a model for the post-glacial evolution of the valley. In particular, it assesses the origins of hummocky topography on the valley oor which, like in many other parts of the world, have previously been interpreted to be glacial in origin. Geomorphic field mapping, GPR, sedimentology (clast and agglomerate identification), and a novel terrestrial cosmogenic nuclide dating (TCND) method of extracting meteoric 10Be from pyroxene minerals were utilised to reconstruct the geomorphology of the valley during the Holocene. Glacial deposits were confirmed at Knobs Flat and Eglinton Flat while RA deposits were conclusively found at Knobs Flat, Deer Flat, and adjacent to Lake Malvora. Eglinton Valley has been completely blocked on (a minimum of) three separate occasions, forming a large lake each time, with only Lake Gunn and a few minor swamps and lakes (e.g. Lake Malvora) remaining today. Relative age dating evidence suggests the first lake was formed by the large Deer Flat RA, the next formed due to the extensive Wesney Creek alluvial fan, and the youngest, Lake Gunn, as a result of the Lake Gunn Landslide ~7.6 kyrs BP. TCND was uncompleted due to lab contamination at the final step, however, the methods attempted here appeared to yield promising results. The Eglinton Valley has been sculpted by glacial, mass movement, and fluvial processes. This work advances the knowledge of the processes responsible for the hummocky terrain found throughout Eglinton Valley, and adds to the currently limited pool of research into the reinterpretation of hummocky deposits within deglaciated valleys in a global and New Zealand context.